Illustrations of the Huttonian Theory of the EarthPlayfair, John
Science
Illustrations of the Huttonian Theory of the Earth
Playfair, John
Geology; Hutton, James, 1726-1797. Theory of the earth
This argument is plausible; but, I think, nevertheless inconclusive.
The sand found in the gold, accounts, at least in part, for its
lightness. It is only by repeated fusions that any of the metals is
brought to its utmost purity and highest specific gravity; and on no
supposition can the melting of gold in the mineral regions, be very
likely to separate it from heterogeneous substances. That quartzy
sand should be found in it, after such a process, is naturally to be
expected. The impressions which the quartz crystals have left on the
Wicklow gold, would be received as a full proof of the fusion of that
metal, if geologists always regulated their theories by the principles
which determine the belief of ordinary men.
217. Don Rubin de Celis, in the paper referred to above, mentions some
masses of silver found at Quantajaia, and also some dust of platina, in
terms that excite a strong desire to have more information concerning
them. They are considered by him as effects of volcanic fire; so we
may conclude, that they contain evident marks of fusion, and would in
this system be ascribed to that heat, from which volcanic fire is but a
partial and accidental derivation.
218. The state also in which gold and silver are often found pervading
masses of quartz, and shooting across them in every direction,
furnishes a strong argument for the igneous origin, both of the metal
and the stone. From such specimens, it is evident, that the quartz
and the metal crystallized, or passed from a fluid to a solid state,
at the same time; and it is hardly less clear, that this fluidity did
not proceed from solution in any menstruum: For the menstruum, whether
water or the _chaotic fluid_, to enable it to dissolve the quartz,
must have had an alkaline impregnation; and, to enable it to dissolve
the metal, it must have had, at the same time, an acid impregnation.
But these two opposite qualities could not reside in the same subject;
the add and alkali would unite together, and, if equally powerful,
form a neutral salt, (like sea-salt,) incapable of acting either on
the metallic or the siliceous body. If the acid was most powerful, the
compound salt might act on the metal, but not at all upon the quartz;
and if the alkali was most powerful, the compound might act on the
quartz, but not at all on the metal. In no case, therefore, could it
act on both at the same time. Fire or heat, if sufficiently intense,
is not subject to this difficulty, as it could exercise its force with
equal effect on both bodies.
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